Nitrogen and phosphorus are universally recognized as limiting elements in the
eutrophication processes affecting the majority of the world's lakes, reservoirs, and coastal …

The traditional carbon accounting method, with a lag of over 2 years due to the release time
of statistical yearbooks, impedes timely policy adjustments in urban planning and …

As the largest reactive organic carbon pool, dissolved organic matter (DOM) plays an
important role in various biogeochemical processes in lake ecosystems. Recently, climate …

Chlorophyll-a (Chl a) is an important indicator of algal biomass frequently used to evaluate
the severity of cultural eutrophication. Identifying the key covariates of Chl a concentrations …

Lakes and reservoirs act as active carbon (C) reactors and regulators. Both play a crucial
terrestrial ecosystem C balance role via carbon dioxide (CO2) exchange processes across …

Wetlands are important carbon sinks. However, the carbon sequestration potential of
flooded wetlands may be weakened owing to water regime changes induced by …

Reservoir carbon cycling is a critical component of the global carbon cycle, particularly in
subtropical canyon-shaped reservoirs where unique geomorphological features and …

Natural lakes are significant global sources of CO 2 emissions; however, data from lakes in
karst regions, which cover 15.2% of the Earth's surface, remain insufficiently categorized …

Lakes are sources of atmospheric carbon dioxide (CO 2), contributing to global climate
change. Temporal variations in lake CO 2 emissions are pronounced, with algal growth and …

Lakes exhibit a biological pump (BP) effect, akin to marine systems, acting as a carbon
sequestration mechanism. In karst lakes, the BP works in synergy with a more efficient …